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Results:

• 21. norsem_lund

  more events in the vicinity in the next two months. These aftershocks are interesting as aftershocks to M4+ events are not always observed in Sweden and Finland. The Bothnian Bay is one of the most seismically active areas in continental Fennoscandia, but the cause of the seismicity is still not well known. Until recently, the offshore areas have been poorly monitored by the national seismic /media/norsem/norsem_lund.pdf

• 22. The Arctic HYCOS group

  of the Arctic. The main objectives of the Arctic HYCOS working group have been developed in parallel with an assessment report prepared by a related collaborative venture, Arctic HYDRA. The report can be downloaded from the Arctic Portal web-site. Freshwater inflow to the Arctic Ocean – contributions of main rivers in cubic kilometers per year. The total annual inflow (4270 km3) is similar /about-imo/news/nr/2447

• 23. OSTIA Sea surface temp.

  < Time - 0Time - 1Time - 2Time - 3Time - 4Time - 5Time - 6Time - 7Time - 8Time - 9Time - 10Time - 11Time - 12 > Load all OSTIA uses satellite data provided by the GHRSST project, together with in-situ /weather/shipping/sea-surface-temperature/ostia/

• 24. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  The well-being of any human community is critically dependent on continued access to natural and man-made resources. Decades before sustainability became a popular slogan, the Ostroms began to investigate the conditions under which natural resources can be man- aged in a sustainable manner. The origins of the Workshop approach can be traced back at least as far as “State Administration of Natural /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 25. Horsens_case

  a narrow shipping channel with a depth between 7 and 22 m. The catchment area is 517 km2 and dominated by agriculture (75%) with small areas of forests, wetlands, lakes and urban areas. The annual freshwater input is in the order of 100 Mm3, where approximately 70% is channelled through two main creaks Bygholm å and Hansted å, located in the inner part of the fjord. Several smaller streams /media/loftslag/Horsens_case.pdf

• 26. Full membership to EUMETSAT

  for the Environment and Natural Resources, Sigurður Ingi Jóhannsson, and the EUMETSAT Director General, Alain Ratier, signed the accession agreement. As a full member state, Iceland will have unlimited access to satellite earth observation data that relates to many aspects of atmospheric, land and ocean monitoring. Furthermore, Iceland in cooperation with other memberstates will now be able to take full /about-imo/news/nr/2733

• 27. Lecture on abrupt changes in summer sea ice extent

  (1979 -2006). The sea ice albedo feedback is often cited as being responsible for the large changes in future sea ice conditions in the Arctic. In this presentation we look at other feedbacks mechanisms involving the atmosphere (clouds) and the ocean in promoting ice free conditions. Simulations from control and forced runs are presented to bring to light the effect of increased greenhouse gas /about-imo/news/nr/1665

• 28. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  Institution BCCR-BCM2.0 Bjerknes Centre for Climate Research, Norway CGCM3.1 (T47) Canadian Centre for Climate Modelling and Analysis CGCM3.1 (T63) same as previous CNRM-CM3 Météo-France CSIRO-MK3.0 CSIRO Atmospheric Research, Australia ECHAM5/MPI-OM Max Planck Institute (MPI) for Meteorology, Germany ECHO-G University of Bonn and Model & Data Group, Germany; Korean Meteorological Agency GFDL /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 29. HaBj_PlumePictures_w_explanations-20140901

  Photos of the eruption plume taken on September 1st 2014 Halldór Björnsson, Icelandic Meteorological Office. TF-SIF an airplane from the Icelandic Coast Guard flew over the volcano and nearby areas in the north of Vatnajökull on September 1st from kl. 13:45 to 16:30. Despite relatively cloudy conditions, the visibility was acceptable, especially at low altitude. This document discusses several /media/jar/myndsafn/HaBj_PlumePictures_w_explanations-20140901.pdf

• 30. Pyroclastic flow

  of the volcano.Because eruption column density is lower than the atmosphere, the column in most cases ascends many kilometres above the volcano. Finally, it spreads out and forms a cloud and the ash coming from the column is dispersed with the wind. However, when the eruption column can't intake enough air it cools down and becomes denser than the surrounding air. When this happens the column collapses /volcanoes/volcanic-hazards/pyroclastic-flow/